Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Diffusion coefficients of low-energy protons upstream of quasi-parallel interplanetary shocks

Conference · · Adv. Space Res.; (United States)
OSTI ID:5823080
Results are presented of a study of the diffusion coefficient for low-energy protons upstream of three interplanetary shocks observed on ISEE-3. The intensity increase as the shock approaches can be fitted by a running exponential, the e-folding time t-asterisk of which is assumed to be a direct measure of the diffusion coefficient. The energy dependence of t-asterisk close to the shock (0-60 Re) is derived from the four energy channels covering the range 35-238 keV. The t-asterisk in the low energy channels (less than 100 keV) increases with distance away from the shock. However t-asterisk decreases above 100 keV and roughly beyond 100 Re, so that the diffusion coefficient becomes independent of energy. It is suggested that the energy-independence of t-asterisk in a region well upstream of the shock is the result of enhanced parallel scattering through 90-deg pitch-angles for higher energy (larger gyroradius) particles which are more sensitive to variations in the transverse direction of the magnetic field. 7 references.
Research Organization:
ESA, Noordwijk, Netherlands
OSTI ID:
5823080
Report Number(s):
CONF-8406167-
Conference Information:
Journal Name: Adv. Space Res.; (United States) Journal Volume: 4
Country of Publication:
United States
Language:
English

Similar Records

Diffusion coefficients of low-energy protons upstream of quasi-parallel interplanetary shocks
Technical Report · Sat Dec 31 23:00:00 EST 1983 · OSTI ID:6607317

Energetic particle diffusion coefficients upstream of quasi-parallel interplanetary shocks
Journal Article · Thu Jun 01 00:00:00 EDT 1989 · Journal of Geophysical Research; (USA) · OSTI ID:5948537

Plasma and energetic particle structure upstream of a quasi-parallel interplanetary shock
Journal Article · Sun Jul 01 00:00:00 EDT 1984 · J. Geophys. Res.; (United States) · OSTI ID:6399616